When two plates collide with enough force, faulting occurs, breaking the crust. Faulting (Apex)
When two plates carrying continental crust collide, the continental crust is too light to subduct beneath the other plate. Instead, the plates crumple and fold, leading to the formation of mountain ranges. This process is known as continental collision.
Breaks in the Earth's crust where plates meet are called plate boundaries. These boundaries are classified into three types: divergent, convergent, and transform boundaries, depending on the motion of the plates.
When tectonic plates collide they often form volcanoes or moutains. But when they slide past each other they create earthquakes...like in Haiti or Japan.
Oceanic crust is denser than continental crust, dense enough to sink into the mantle. Continental crust is not dense enough to do this.
When two plates collide with enough force, faulting occurs, breaking the crust. Faulting (Apex)
When two plates collide with enough force, faulting occurs, breaking the crust. Faulting (Apex)
When two plates collide with enough force to break the crust, it can lead to the formation of mountain ranges through the process of crustal deformation and uplift. This collision can also create intense seismic activity, such as earthquakes, as the plates interact and adjust to the intense pressure and stress. Additionally, volcanic activity may occur where magma from the mantle is forced up to the surface.
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When continental plates collide, the denser oceanic crust is usually subducted beneath the less dense continental crust. This process can create subduction zones, where the oceanic crust is forced downward into the mantle. The oceanic crust may melt or be recycled back into the mantle in these subduction zones.
When two plates carrying continental crust collide, the continental crust is too light to subduct beneath the other plate. Instead, the plates crumple and fold, leading to the formation of mountain ranges. This process is known as continental collision.
When two plates collide, or come together, the plates will push upward, forming a mountain. If one plate is continental crust and the other is oceanic crust, the less dense crust (this being the oceanic) will actually move under the more dense crust, in a process called subduction, to form a deep-ocean trench.
Yes, faults are breaks in the Earth's crust where plates meet. These breaks allow movement to occur along the plate boundaries, resulting in earthquakes as the plates slide past each other.
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Breaks in the Earth's crust where plates meet are called plate boundaries. These boundaries are classified into three types: divergent, convergent, and transform boundaries, depending on the motion of the plates.
Yes, it "dives" under the continental crust and back into the mantle.
tectonic plates under the earth's crust collide or rub against each other